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Generating a Comprehensive Climate Change Streamflow Scenarios
Database for the Columbia River Basin
Alan F. HamletKurt Unger Philip W. MoteEric SalathéDennis P. Lettenmaier
JISAO/CSES Climate Impacts GroupDept. of Civil and Environmental EngineeringUniversity of WashingtonWA State Department of Ecology
Image Credit: National Snow and Ice Data Center, W. O. Field, B. F. Molniahttp://nsidc.org/data/glacier_photo/special_high_res.html
Aug, 13, 1941 Aug, 31, 2004
Recession of the Muir Glacier
March 5, 2002
Collapse of theLarsen B Ice shelf,Antarctica
Mote P.W.,Hamlet A.F., Clark M.P., Lettenmaier D.P., 2005, Declining mountain snowpack in western North America, BAMS, 86 (1): 39-49
Trends in April 1 SWE 1950-1997
Overview of 21st Century Climate Projections and Some Water Resources Impact Pathways
Pacific Northwest
°C
0.4-1.0°C0.9-2.4°C 1.2-5.5°C
Obse
rved 2
0th
centu
ry v
ari
abili
ty
+1.7°C+0.7°C
+3.2°C
Pacific Northwest
% -1 to +3%
-1 to +9% -2 to +21%
Obse
rved 2
0th
centu
ry v
ari
abili
ty
+1% +2%
+6%
0
20
40
60
80
100
120
oct nov dec jan feb mar apr may jun jul aug sep
Sim
ula
ted
Bas
in A
vg R
un
off
(m
m)
1950
plus2c
Simulated Changes in Natural Runoff Timing in the Naches River Basin Associated with 2 C Warming
Impacts:•Increased winter flow•Earlier and reduced peak flows•Reduced summer flow volume•Reduced late summer low flow
Water Supply and Demand
•Changes in the seasonality water supply (e.g. reductions in summer)
•Changes in water demand (e.g. increasing evaporation)
•Changes in drought stress
•Increasing conflicts between water supply and other uses and users of water
Energy Supply and Demand
•Changes in the seasonality and quantity of hydropower resources
•Changes in energy demand
•Increasing conflicts between hydro and other uses and users of water
Instream Flow Augmentation
•Changes in low flow risks
•Changes in the need for releases from storage to reproduce existing streamflow regime.
•Changes in water resources management related to water quality (e.g. to provide dilution flow or to control temperature)
Flood Control and Land Use Planning
•Changes in flood risks
•Changes in flood control evacuation and timing
•Dam safety
Impacts in Estuaries
•Impacts of sea level rise and changing flood risk on low lying areas (dikes and levies)
•Impacts to ecosystem function
•Changes in land use policy (coastal armoring, land ownership, FEMA maps)
Long-Term Planning, Water Resources Agreements, Water Law and Policy
•Water allocation agreements in a non-stationary climate (e.g. water permitting)
•Appropriateness of the historic streamflow record as a legal definition of climate variability
•Need for new planning frameworks in a non-stationary climate
•Transboundary implications for the Columbia Basin
As the public and professionals in the water management and policy arenas have become increasing concerned about the impacts of climate change on PNW water resources, demand for hydrologic scenarios suitable for planning purposes at a range of spatial scales has increased dramatically.
Currently there does not exist an up-to-date, comprehensive, and self-consistent data base of hydrologic scenarios for the Columbia River basin that is suitable for the range of planning activities the Climate Impacts Group is being asked to support.
A Need to Provide Improved Access to Hydrologic Scenarios for Planning
Study Overview
Collaboration with WA Department of Ecology and Regional Stakeholders to Provide Improved Access to Hydrologic Scenarios in the Columbia River Basin
Funding Source: House Bill 2860
•$16 Million for studies related to enhancing water supplies in the Columbia River basin for irrigation and municipal water supply.
•Up to $200 Million for implementing improvements identified by these studies.
Answers to FAQ regarding WA 2860 from the Department of Ecology website:
http://www.ecy.wa.gov/pubs/0611014.pdf
Regional Study Partners
•WA State Department of Ecology
•Bonneville Power Administration
•Northwest Power and Conservation Council
•State of Oregon
•Province of British Columbia (BC Hydro and The Ministry of Environment)
Streamflow Data Needs to Support a 21st Century Planning Framework Incorporating Climate Information and Uncertainty
2 Emissions Scenarios
20 GCM Scenarios
2 Downscaling Approaches
X
X
2 Hydro. Modeling ApproachesX
= Up to 160 realizations of future streamflow variability at each location!
The Need to Encompass Multiple Spatial Scales
Large Scale Planning Studies
Examples:
•Hydro System Performance•Flood Control•Main Stem ESA•Transboundary Issues•Large-Scale Irrigation Impacts
WA State Water Resources Inventory Areas
Medium Scale Planning Studies
Examples:
Water Supply Planning
•Yakima Basin•Okanogan Basin•Methow•Walla Walla Basin
Snow Model
Schematic of VIC Hydrologic Model and Energy Balance Snow Model
PNW1/16th
Deg.
6 km
6 km
Alternate Approach: DHSVMDeveloped in the
UW Land Surface
Hydrology Research
Group at UW, the model has been used for over a decade in hydrologic research applications associated with small catchments.
DHSVM: Distributed Hydrology-Soil-Vegetation Model
Blue = Large Scale Planning Sites
Green = Snake River Sites
Red = Additional Sites in WA
Partnerships with the BPA, NWPCC, OR and BC will extend the number of sites included in the study to support specific planning activities in these areas. The UW will also collaborate informally with the U of I.
Streamflow Locations Currently Under Consideration
On-Line Survey Website, Project Scope
http://cses.washington.edu/cig/http://www.surveymonkey.com/s.aspx?sm=daSOYBVOb238oFy6ia7bcA_3d_3d